
sedimentary
Conglomerate (River Rock Aggregate)
Conglomerate (Lithic-clast conglomerate)
Hardness: Variable (6-7 for quartz clasts); Color: Multicolored (brown, grey, reddish, black); Luster: Dull to earthy; Structure: Clastic, consisting of rounded to sub-angular pebbles embedded in a fine-grained matrix/cement; Cleavage: None.
- Hardness
- Variable (6-7 for quartz clasts)
- Color
- Multicolored (brown, grey, reddish, black)
- Luster
- Dull to earthy
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Physical properties
Hardness: Variable (6-7 for quartz clasts); Color: Multicolored (brown, grey, reddish, black); Luster: Dull to earthy; Structure: Clastic, consisting of rounded to sub-angular pebbles embedded in a fine-grained matrix/cement; Cleavage: None.
Formation & geological history
Formed by the accumulation and subsequent lithification of rounded water-worn rock fragments. These are typically deposited in high-energy environments like riverbeds, alluvial fans, or beaches. The age can range from Recent to billions of years old.
Uses & applications
Used primarily in the construction industry as decorative aggregate, building stone (as seen in the mural/wall in the image), and as road base material. Occasionally used as an architectural veneer.
Geological facts
Conglomerate is often called a 'puddingstone' because it looks like a pudding filled with raisins and nuts. Famous examples include the Roxbury Conglomerate in Massachusetts. It is technically more of a 'rock type' than a single mineral.
Field identification & locations
Identify in the field by looking for rounded pebbles (clasts) larger than 2mm that are clearly cemented together by a finer material. Found globally in ancient riverbeds or mountain-front deposits. For collectors, look for unique colors or jasper-rich clasts.
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